地球科学进展 ›› 2009, Vol. 24 ›› Issue (9): 1009 -1014. doi: 10.11867/j.issn.1001-8166.2009.09.1009

研究论文 上一篇    下一篇

牛向龙 1,2,李江海 2,冯  军 2,3   
  1. 1.中国地震局地质研究所,北京   100029;  2.北京大学地球与空间科学学院,北京  100871;  3.中国地震局应急搜救中心,北京  100049
  • 收稿日期:2009-02-04 修回日期:2009-07-20 出版日期:2009-09-10
  • 通讯作者: 牛向龙 E-mail:xlniu01@yahoo.com.cn
  • 基金资助:


Origin of the Neoarchean Massive Sulphide Deposits in Wutaishan Mt: An indication for the Submarine Exhalation from the Microstructures

Niu Xianglong 1,2, Li Jianghai 2, Feng Jun 2,3   

  1. 1.Institute of Geology, Chinese Earthquake Administration, Beijing 100029, China;
    2.School of Earth and Space, Peking University, Beijing 100871, China;
    3.National Earthquake Response Support Service, China Earthquake Administration, Beijing 100049,China
  • Received:2009-02-04 Revised:2009-07-20 Online:2009-09-10 Published:2009-09-10
  • Contact: Niu Xianglong E-mail:xlniu01@yahoo.com.cn


     Some specimens of porous sulphide ore are found in the Neoarchean massive sulphide deposits in Jingangku, Wutaishan Mt. Based on the results of the detailed microscopic observition and the analysis of electron probe to the samples, the similar textures and structures, as colloform texture, channel structure, filling structure, zonal structure and so on, with the modern seafloor sulphide chimney are identified. These samples are thought as the relics of the Neoarchean seafloor sulphide black chimneys owing to the above reasons, which indicate the originese of the Jingangku sulphide ore maybe contribute to the submarine exhalative model.


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